<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>1405-3322</journal-id>
<journal-title><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. Soc. Geol. Mex]]></abbrev-journal-title>
<issn>1405-3322</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Geológica Mexicana A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-33222023000300112</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2023v75n3a240823</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Morphometry of the Samalayuca dunes, northern Chihuahua, Mexico]]></article-title>
<article-title xml:lang="es"><![CDATA[Morfometría de las dunas de Samalayuca, norte de Chihuahua, México]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Domínguez-Acosta]]></surname>
<given-names><![CDATA[Miguel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Langford]]></surname>
<given-names><![CDATA[Richard P.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gill]]></surname>
<given-names><![CDATA[Thomas E.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma de Ciudad Juárez Departamento de Ingeniería Civil y Ambiental ]]></institution>
<addr-line><![CDATA[Ciudad Juárez Chihuahua]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,The University of Texas at El Paso Environmental and Resource Sciences Department of Earth]]></institution>
<addr-line><![CDATA[El Paso Texas]]></addr-line>
<country>USA</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<volume>75</volume>
<numero>3</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222023000300112&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222023000300112&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222023000300112&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The Samalayuca Dunes (SMD) (Médanos de Samalayuca), Chihuahua, México, are one of México&#8217;s largest and least studied dune fields, now managed as a Protected Area for their ecological characteristics. We present a morphometric characterization of the dune field based on remote sensing and field studies, to advance understanding of its physical environment. SMD&#8217;s generally-fine sands originate from shoreline deposits of Paleolake Palomas, transported eastward (downwind) along an aeolian corridor, accumulating primarily as echo dunes upwind of the sierras of Samalayuca and Presidio. A complex wind regime, with northerly and southerly winds complementing regionally-prevailing southwesterlies, modified by topographic effects, shapes the SMD&#8217;s morphology. The sand sea covers ~139.7 km2, with ~113.8 km2 in the main eastern body and ~25.9 km2 in a northwestern subfield. We describe six major dune forms: north to south straight-crested dunes, east to west straight-crested dunes, star dunes, vegetated parabolic dunes, relict transverse dunes, and &#8220;megastar&#8221; (draa) dunes. Mean interdune centroid spacing is 76.5 m. The active dunes, previously described as an &#8220;aklé&#8221; pattern, are predominantly straight-crested dune sets oriented near-perpendicular to each other with general north-south and east-west crest orientations, 4-5 m high, spaced ~67 m apart for north-south trending crests and ~53 m for east-west trending crests, representing a nearly perpendicular interference pattern in some locations. The active dunes are superimposed in a compound and complex arrangement on relict remnants of much larger north-northwest trending transverse dune ridges fanning out from south to north-northwest, spaced approximately ~1 km apart and ~50 m high. The easternmost dune ridge contains an active set of at least 15 active megastar and reversing dunes up to 120 m tall, increasing in size and complexity from south to north. As a protected area with historical and ecological value, additional geologic investigations should be performed at the SMD, to help conserve this remarkable geologic feature.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Las Dunas o Médanos de Samalayuca se localizan en el estado de Chihuahua, México, y forman parte de uno de los ergs más grandes y menos estudiados en México, y que actualmente se encuentran designadas como área de protección de flora y fauna. Este estudio presenta una caracterización morfométrica del campo de dunas, basada en datos de campo y sensores remotos, con la intención de establecer la base de entendimiento de este sistema. Sus sedimentos en tamaño de arenas finas tienen origen en los depósitos de litoral del Paleo-lago Pluvial Palomas, son transportados rumbo al este a través de un corredor eólico y depositados principalmente como dunas tipo eco en el margen oeste de las sierras de Samalayuca y del Presidio. Su morfología está influenciada por un régimen complejo de vientos provenientes del norte y del sur, los cuales complementan a los vientos prevalentes en la región provenientes del suroeste, además de los efectos topográficos impuestos por las sierras cercanas. Las dunas cubren una superficie de ~139.7 km2, de los cuales, el cuerpo principal abarca ~113.8 km2, mientras que el menor un área aproximada de ~25.9 km2. Se describen seis tipos principales de dunas: dunas de crestas rectilíneas orientadas norte a sur, dunas de crestas rectilíneas orientadas este a oeste, dunas estrella, dunas parabólicas vegetadas, dunas transversales relictas y, dunas &#8220;megaestrella&#8221; o draa. El espaciamiento promedio del centroide de interdunas es de 76.5 m. Las dunas activas más abundantes están formadas por juegos de dunas rectilíneas, orientadas de forma cuasi-perpendicular entre ellas, con orientación general de crestas norte-sur y este-oeste, una altura promedio de 4 a 5 m y, un espaciamiento promedio de ~67 m para las crestas norte-sur y ~53 m para las crestas este-oeste. Estas dunas previamente descritas como &#8220;aklé&#8221;, son en realidad resultado de un patrón de interferencia cuasi-perpendicular. Las dunas activas sobreyacen de forma compuesta y compleja a los remanentes relictos de cordilleras de megadunas transversales orientadas NNO, las cuales presentan un espaciamiento promedio de ~1 km y altura de ~50 m. La cordillera de mayor relieve presenta un grupo de aproximadamente 15 dunas activas de tipo megaestrella e inversas de hasta 120 m de altura, las cuales incrementan en tamaño y complejidad de sur a norte. Acorde con su estatus de área de protección ecológica y su gran valor geológico e histórico, es necesario continuar con la investigación que permita garantizar la preservación este imponente y bello monumento geológico.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[dunes]]></kwd>
<kwd lng="en"><![CDATA[sand]]></kwd>
<kwd lng="en"><![CDATA[aeolian processes]]></kwd>
<kwd lng="en"><![CDATA[Samalayuca]]></kwd>
<kwd lng="en"><![CDATA[Chihuahua]]></kwd>
<kwd lng="es"><![CDATA[dunas]]></kwd>
<kwd lng="es"><![CDATA[arena]]></kwd>
<kwd lng="es"><![CDATA[procesos eólicos]]></kwd>
<kwd lng="es"><![CDATA[Samalayuca]]></kwd>
<kwd lng="es"><![CDATA[Chihuahua]]></kwd>
</kwd-group>
</article-meta>
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